地壳和地幔介质的流变断裂实验研究是地球动力学研究中的重要一环。地壳中能量的积累和地球动力过程的驱动力等许多问题,用线性模型来分析已经不够了,需要发展介质的非线性理论,以建立较符合实际的物理模型。高温高压实验是有助于建立这种物理模型的重要手段。岩石高温高压实验方面的工作,国际上已有半个多世纪的历史。有许多国家,许多单位,以各种特点进 The rheological fracture experimental study of the crust and mantle media is an important part of the geodynamics study. Many problems such as the accumulation of energy in the Earth’s crust and the driving force of the Earth’s dynamic process, etc., have not been analyzed by the linear model. It is necessary to develop the nonlinear theory of the medium to establish a more realistic physical model. High temperature and high pressure experiments are important means to help establish this physical model. The work on rock high-temperature and high-pressure experiments has been internationally more than half a century old. There are many countries, many units, with various characteristics